| 000 | 00000cam 2200000zi 4500 |
| 001 | 9.959172 |
| 003 | CaOODSP |
| 005 | 20260122132617 |
| 006 | m o d f |
| 007 | cr |n||||||||| |
| 008 | 260121t20142014oncdab ob f|0| 0 eng d |
| 040 | |aCaOODSP|beng|erda|cCaOODSP |
| 043 | |an-cn-mb |
| 086 | 1 |aM183-2/7590E-PDF |
| 100 | 1 |aCraven, James A. |q(James Allan), |d1963- |eauthor. |
| 245 | 10|aDetails and preliminary positive evaluation of a test seismic interferometry survey at an active VMS mine near Snow Lake, Manitoba / |cJ.A. Craven, S. Cheraghi, B.J. Roberts, G. Bellefleur, E. Schetselaar, D. Melanson, B. Bancroft, and K. Miah. |
| 264 | 1|a[Ottawa] : |bGeological Survey of Canada, |c2014. |
| 264 | 4|c©2014 |
| 300 | |a1 online resource (30 pages) : |bcharts, illustrations, maps. |
| 336 | |atext|btxt|2rdacontent |
| 337 | |acomputer|bc|2rdamedia |
| 338 | |aonline resource|bcr|2rdacarrier |
| 490 | 1 |aOpen file, |x2816-7155 ; |v7590 |
| 504 | |aIncludes bibliographical references (pages 20-22). |
| 520 | |a"Seismic reflections methods are a powerful tool to detect and image structures associated with volcanogenic massive sulphide (VMS) deposits. Seismic interferometry has recently been developed as a robust method to process passive seismic data and image geological features. In order to test the capability of seismic interferometry to image ore deposits in the crystalline rock environment approximately 300 hours of ambient noise data covering an area of 4 km² were acquired over the Lalor mining area, near Snow Lake, MB, Canada"--Abstract, page 4. |
| 650 | 0|aSeismic reflection method. |
| 650 | 0|aInterferometry. |
| 650 | 6|aMéthode sismique-réflexion. |
| 650 | 6|aInterférométrie. |
| 710 | 2 |aGeological Survey of Canada, |eissuing body. |
| 830 | #0|aOpen file (Geological Survey of Canada)|v7590.|w(CaOODSP)9.506878 |
| 856 | 40|qPDF|s1.82 MB|uhttps://publications.gc.ca/collections/collection_2026/rncan-nrcan/m183-2/M183-2-7590-eng.pdf |
| 856 | 4 |qHTML|sN/A|uhttps://doi.org/10.4095/293669 |